{"title":"寒武纪-奥陶纪伊比利亚西北部主动边缘向被动边缘转变的同位素和地球化学记录:大陆弧衰落的遗迹","authors":"P. Andonaegui, R. Díez Fernández, J. Abati","doi":"10.1007/s41513-020-00155-8","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":54799,"journal":{"name":"Journal of Iberian Geology","volume":"47 1","pages":"323 - 346"},"PeriodicalIF":1.3000,"publicationDate":"2021-01-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1007/s41513-020-00155-8","citationCount":"2","resultStr":"{\"title\":\"Isotopic and geochemical record of the active to passive margin transition in NW Iberia during the Cambrian-Ordovician: vestiges of a waning continental arc\",\"authors\":\"P. Andonaegui, R. Díez Fernández, J. Abati\",\"doi\":\"10.1007/s41513-020-00155-8\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":54799,\"journal\":{\"name\":\"Journal of Iberian Geology\",\"volume\":\"47 1\",\"pages\":\"323 - 346\"},\"PeriodicalIF\":1.3000,\"publicationDate\":\"2021-01-05\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1007/s41513-020-00155-8\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Iberian Geology\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1007/s41513-020-00155-8\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Iberian Geology","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1007/s41513-020-00155-8","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOLOGY","Score":null,"Total":0}
Isotopic and geochemical record of the active to passive margin transition in NW Iberia during the Cambrian-Ordovician: vestiges of a waning continental arc
期刊介绍:
The Journal of Iberian Geology will consider for publication original, high-quality papers (including research articles, reviews and brief communications) dealing with different aspects of Earth Sciences in Latin America and the Caribbean, as well as the Mediterranean region, including Geology, Paleontology, Geophysics and Geochemistry. The journal welcomes research papers with regional appeal, but these should present results of international interest. The Journal accepts collections of selected original papers on topics within these scopes, which will be published as edited monographic issues.